2008
DOI: 10.1080/00222930802105130
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Did dinosaurs have any relation with dung‐beetles? (The origin of coprophagy)

Abstract: It is widely accepted that Mesozoic ecosystems were basically similar to Cenozoic ecosystems and it has been proposed that the role of dung-beetles in those ecosystems was identical to that of today, but the dung of dinosaurs were used as a source of food instead of the dung of mammals. While dinosaurs have been known since Triassic, Scarabeids are present in the fossil records probably since Lower Jurassic. But a very important metabolic feature of dinosaurs has not been taken into account, the connection bet… Show more

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Cited by 19 publications
(10 citation statements)
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“…Trace fossils within herbivorous dinosaur coprolites attributed to tunneling dung beetles appear in the Upper Cretaceous, the oldest from the Campanian [ 72 , 76 ], younger than the oldest Scarabaeinae fossil ( Prionocephale deplanate Lin)[ 33 ]. Conversely, it has been argued that the mixing of uric acid with feces common to all non-mammals would have made dinosaur dung unsuitable [ 77 ], a hypothesis supported by the rarity of extant dung beetles utilizing reptile or avian dung. Molecular-clock based estimates for the crown age of marsupials and placental mammals are as old as 82 and 101Ma, with peak mammal diversification between 75-85Ma [ 78 ].…”
Section: Discussionmentioning
confidence: 99%
“…Trace fossils within herbivorous dinosaur coprolites attributed to tunneling dung beetles appear in the Upper Cretaceous, the oldest from the Campanian [ 72 , 76 ], younger than the oldest Scarabaeinae fossil ( Prionocephale deplanate Lin)[ 33 ]. Conversely, it has been argued that the mixing of uric acid with feces common to all non-mammals would have made dinosaur dung unsuitable [ 77 ], a hypothesis supported by the rarity of extant dung beetles utilizing reptile or avian dung. Molecular-clock based estimates for the crown age of marsupials and placental mammals are as old as 82 and 101Ma, with peak mammal diversification between 75-85Ma [ 78 ].…”
Section: Discussionmentioning
confidence: 99%
“…These ancestral lineages of Aphodiinae possibly had different feeding (mycetophagy or saprophagy; Scholtz & Chown, 1995) and ecological habits (forest‐ or sand‐dwellers), as has been observed previously within earlier branches of Iberian Aphodiinae, which show proportionally more of these tendencies than more recent groups (Cabrero‐Sañudo & Zardoya, 2004; Cabrero‐Sañudo, 2007). Although there are no fossil records for Aphodiinae from this period (Krell, 2003), the radiation of coprophagous beetles presumably happened as a response to an increasing rate of dung production, density and size of vertebrate droppings from dinosaurs and/or small mammals (Jeannel, 1942; Halffter & Matthews, 1966; Davis, 1990; Arillo & Ortuño, 2008), as is thought to have happened in the case of the sister group Scarabaeinae (Davis et al. , 2002).…”
Section: Discussionmentioning
confidence: 99%
“…Probably an important feature of dinosaur and pterosaur excrements (as in birds and reptiles when compared with mammals) was the large proportion of nitrogen compared with phosphorus [16] . The association with urine and thus with a high concentration of phosphoric acid, oxalic and carbonic acids and salts, primarily sodium chloride, leads to the recent conclusion about the association of dung-beetles and coprophagy with mammals (not with dinosaurs) since the very beginning [17] . On the other hand, some common (11 of the 15 deposits) fossilised dinosaur coprolites contain 13–85% of rotting conifer wood with only 0.20–0.30% of nitrogen (conifers are utilized by the living cockroach Cryptocercus – the most important wood-decomposing cockroach) with its attendant microbial and detritivore fauna and thus augmented the resource options of Cretaceous ecosystems that lacked fodder provided by grasses and other derived angiosperms [8] , [18] .…”
Section: Introductionmentioning
confidence: 99%